Published September 26, 2014 | Version v1
Taxonomic treatment Open

Psilochara acuta Grambast & Paul 1965

Description

Psilochara aff. acuta Grambast & Paul, 1965

(Fig. 6 E-H)

Psilochara acuta Grambast & Paul, 1965: 243, pl. 2, fig. 5-9.

DISTRIBUTION. — Psilochara acuta has been recorded from many localities in Europe. In France, this species has been reported in the Lower Oligocene (Rupelian) of the Paris Basin (Riveline 1986). Schwarz (1997) recorded this species from the Oligocene of the Rhine Graben (Germany). Psilochara acuta was later reported from Upper Eocene (Priabonian) beds in the Transylvanian Basin, Romania by Baciu & Hartenberger (2001). Ŋe occurrence of this species in the Ebro Basin (Sarral locality) represents its southernmost record (Table 4). Riveline (1986) showed that the biostratigraphic range of this species encompasses three charophyte biozones i.e. Lychnothamnus pinguis, Lychnothamnus major and Chara microcera. However, the occurrence of this species within the European Harrisichara vasiformis-tuberculata biozone in the Transylvanian Basin and within the Lychnothamnus vectensis biozone in the Ebro Basin suggests that the occurrence of Psilochara aff. acuta starts in the middle part of the Priabonian.

DESCRIPTION

Gyrogonites small to medium, 360-549 µm high (mean 478 µm) and 280-450 µm wide (mean 327 µm), prolate and elongate in shape, with an isopolarity index ranging from 103-184 (mean 147). Spiral cells flat to concave, about 53 µm wide and without ornamentation. Eight to ten (frequently nine) convolutions are visible in lateral view. Apex psilocharoid and prominent, frequently pointed. Ŋis apical cap is very variable in size, ranging between 15 and 77 µm in high. Base rounded in well-calcified gyrogonites and slightly pointed in poorly calcified gyrogonites, showing a small pentagonal pore (about 40 µm in diameter).

REMARKS

Ŋe main difference between the population from Sarral (NE Ebro Basin) and the type material from Soisy-sur-École (Paris Basin) is the size of the gyrogonites, which is about 250 µm smaller in the Ebro Basin. Moreover, gyrogonites from the type population display a larger range of convolutions (eight to twelve).

Notes

Published as part of Sanjuan, Josep & Martín-Closas, Carles, 2014, Taxonomy and palaeobiogeography of charophytes from the Upper Eocene- Lower Oligocene of the Eastern Ebro Basin (Catalonia, NE Spain), pp. 385-420 in Geodiversitas 36 (3) on page 396, DOI: 10.5252/g2014n3a3, http://zenodo.org/record/4538531

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Linked records

Additional details

Biodiversity

Family
Characeae
Genus
Psilochara
Kingdom
Plantae
Order
Charales
Phylum
Charophyta
Scientific name authorship
Grambast & Paul
Species
acuta
Taxon rank
species
Taxonomic concept label
Psilochara acuta Grambast, 1965 sec. Sanjuan & Martín-Closas, 2014

References

  • GRAMBAST L. & PAUL P. 1965. - Observations nouvelles sur la flore de charophytes du Stampien du bassin de Paris. Bulletin de la Societe Geologique de France 7: 239 - 247.
  • RIVELINE J. 1986. - Les Charophytes du Paleogene et du Miocene inferieur d'Europe Occidentale. Cahiers de Paleontologie, Centre National de la Recherche Scientifique, 227 p.
  • SCHWARZ J. 1997. - Charophyten aus dem Tertiar des Oberrheingrabens (Mitteleozan-Untermiozan). Palaeontographica Abt. B 243: 1 - 84.
  • BACIU C. & HARTENBERGER J. L. 2001. - Un exemple de correlation marin-continental dans le Priabonien de Roumanie. Remarques sur la Grande Coupure. Comptes-rendus de l'Academie des Sciences 333: 441 - 446.